まとめ
グリーンランドとヨーロッパの間の火山の裂け目が 深い炭素を放出し 5千6百万年前の温室現象を引き起こしました この発見は古代の気候変動と 地球の深い過程を結びつけています
科学分野:
- 地質学
- 古代気候学
- 地化学
背景:
- パリオセーヌ・エオセーヌ熱極 (PETM) は,約5600万年前の急速な地球温暖化期であった.
- PETMで放出された炭素の様々な源を調べました 火山からの放出ガスやメタン水素を含みます
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